Yes. This metamorphic rock can be made from granite; wavy bands of dark and light layers.
As granite is an igneous material, it would have to undergo a melt, taking away any form it has, such as cleavage. However, in a granite dike, the outer layer of the granite will be a chilled margin, giving it a glassy outer layer.
Bands.
No. Gneiss has foliation in the form of alternating light and dark bands.
Conglomerate is a clastic sedimentary rock that has rounded pebbles included among its clasts. Gneiss is a high-grade foliate metamorphic rock characterized by alternating light and dark bands. It forms from the metamorphism of granite or schist.
schist and gneiss arefoliated and in gneiss you can see the bands.
Gneiss
As granite is an igneous material, it would have to undergo a melt, taking away any form it has, such as cleavage. However, in a granite dike, the outer layer of the granite will be a chilled margin, giving it a glassy outer layer.
Bands.
foliated rocks, defined as "metamorphic rocks with parralel layers or "bands". three examples of these foliated rocks are gneiss, slate, and schist. three examples of foliated rocks are schist, gneiss, and schist.
A rock with minerals aligned into bands or layers.
No. Gneiss has alternating light and dark bands.
Bearing in mind that Gneiss is not a mineral, and that it is very hard, Gneiss does not leave a streak, but scratches the plate (don't try it - this is not how you classify Gneiss). Gneiss is classified by its Gneissose Banding - distinct bands of light Feldspar/Quartz and dark Micas. It is also classified by the extent of metamorphism which has taken place.
No. Gneiss has foliation in the form of alternating light and dark bands.
Conglomerate is a clastic sedimentary rock that has rounded pebbles included among its clasts. Gneiss is a high-grade foliate metamorphic rock characterized by alternating light and dark bands. It forms from the metamorphism of granite or schist.
schist and gneiss arefoliated and in gneiss you can see the bands.
Folliated Metamorphic Rock. Example is Gneiss (Banded Gneiss)
Gneiss is formed from pre-existing rocks that are subjected to intense directional pressure and heat, causing an alignment of their constituent minerals into parallel bands, a texture that is referred to as foliation.